Peduruhewa H. Jeewani , Robert W. Brown , Chris D. Evans , Jack Cook , Benjamin P. Roberts , Mariecia D. Fraser , David R. Chadwick , Davey L. Jones
{"title":"再湿润以及添加生物炭和硫酸盐可以减轻温室气体排放,并在退化的高地泥炭地中保留碳","authors":"Peduruhewa H. Jeewani , Robert W. Brown , Chris D. Evans , Jack Cook , Benjamin P. Roberts , Mariecia D. Fraser , David R. Chadwick , Davey L. Jones","doi":"10.1016/j.soilbio.2025.109814","DOIUrl":null,"url":null,"abstract":"<div><div>Peat soils store significant amounts of carbon (C) globally, and increased C sequestration into peatlands could play a role in offsetting anthropogenic greenhouse gas (GHG) emissions. As such, there is a need to find and assess optimal greenhouse gas removal (GGR) interventions to minimise GHG losses, protect current C stocks, and promote further C sequestration. This mesocosm study assessed the additional C storage potential of different <em>C</em>-rich substrates (<em>Juncus</em> straw or <em>Juncus</em>-derived biochar) and/or FeSO<sub>4</sub> amendments, with a low water table (LW; −15 cm) and high-water table (HW; 0 cm) in intact soil columns (20 cm diam. x 25 cm deep) extracted from degraded upland peat. GHG fluxes, soluble nutrients, changes in microbial community structure and enzyme activity were measured over a one-year period to evaluate the net C storage and their overall GGR potential. HW reduced CO<sub>2</sub> emissions by 28 % compared to LW, while CH<sub>4</sub> emissions increased, ultimately contributing 61 % of the overall CO<sub>2</sub> equivalent (CO<sub>2</sub>eq) GHG emissions in HW cores with no amendments. Organic amendments had a significant effect on CO<sub>2</sub> and CH<sub>4</sub> emissions with the highest cumulative emissions being from the Straw-HW (26.2 t CO<sub>2</sub>eq ha<sup>−1</sup> yr<sup>−1</sup>) and the lowest cumulative emissions being from the Biochar + FeSO<sub>4</sub>+HW (7.9 t CO<sub>2</sub>eq ha<sup>−1</sup> yr<sup>−1</sup>). Biochar + FeSO<sub>4</sub>+HW led to the strongest net gain in soil C, suppressing decomposition of the native peat-C as well as CH<sub>4</sub> emissions. The application of FeSO<sub>4</sub> significantly reduced CO<sub>2</sub>eq GHG emissions by preventing methanogenesis through alternative electron acceptors. The Biochar + HW treatment suppressed Ascomycota abundance by 22 %. The combination of a high-water level, biochar addition and availability of alternative electron acceptors (e.g., FeSO<sub>4</sub>) can increase net C accumulation and GGR via both abiotic and biotic mechanisms, including i) increased C input, ii) modulation of soil microbiome to reduce peat turnover; and iii) suppression of CH<sub>4</sub> and N<sub>2</sub>O emissions.</div></div>","PeriodicalId":21888,"journal":{"name":"Soil Biology & Biochemistry","volume":"207 ","pages":"Article 109814"},"PeriodicalIF":9.8000,"publicationDate":"2025-04-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rewetting alongside biochar and sulphate addition mitigates greenhouse gas emissions and retain carbon in degraded upland peatlands\",\"authors\":\"Peduruhewa H. Jeewani , Robert W. Brown , Chris D. Evans , Jack Cook , Benjamin P. Roberts , Mariecia D. Fraser , David R. Chadwick , Davey L. Jones\",\"doi\":\"10.1016/j.soilbio.2025.109814\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Peat soils store significant amounts of carbon (C) globally, and increased C sequestration into peatlands could play a role in offsetting anthropogenic greenhouse gas (GHG) emissions. As such, there is a need to find and assess optimal greenhouse gas removal (GGR) interventions to minimise GHG losses, protect current C stocks, and promote further C sequestration. This mesocosm study assessed the additional C storage potential of different <em>C</em>-rich substrates (<em>Juncus</em> straw or <em>Juncus</em>-derived biochar) and/or FeSO<sub>4</sub> amendments, with a low water table (LW; −15 cm) and high-water table (HW; 0 cm) in intact soil columns (20 cm diam. x 25 cm deep) extracted from degraded upland peat. GHG fluxes, soluble nutrients, changes in microbial community structure and enzyme activity were measured over a one-year period to evaluate the net C storage and their overall GGR potential. HW reduced CO<sub>2</sub> emissions by 28 % compared to LW, while CH<sub>4</sub> emissions increased, ultimately contributing 61 % of the overall CO<sub>2</sub> equivalent (CO<sub>2</sub>eq) GHG emissions in HW cores with no amendments. Organic amendments had a significant effect on CO<sub>2</sub> and CH<sub>4</sub> emissions with the highest cumulative emissions being from the Straw-HW (26.2 t CO<sub>2</sub>eq ha<sup>−1</sup> yr<sup>−1</sup>) and the lowest cumulative emissions being from the Biochar + FeSO<sub>4</sub>+HW (7.9 t CO<sub>2</sub>eq ha<sup>−1</sup> yr<sup>−1</sup>). Biochar + FeSO<sub>4</sub>+HW led to the strongest net gain in soil C, suppressing decomposition of the native peat-C as well as CH<sub>4</sub> emissions. The application of FeSO<sub>4</sub> significantly reduced CO<sub>2</sub>eq GHG emissions by preventing methanogenesis through alternative electron acceptors. The Biochar + HW treatment suppressed Ascomycota abundance by 22 %. 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Rewetting alongside biochar and sulphate addition mitigates greenhouse gas emissions and retain carbon in degraded upland peatlands
Peat soils store significant amounts of carbon (C) globally, and increased C sequestration into peatlands could play a role in offsetting anthropogenic greenhouse gas (GHG) emissions. As such, there is a need to find and assess optimal greenhouse gas removal (GGR) interventions to minimise GHG losses, protect current C stocks, and promote further C sequestration. This mesocosm study assessed the additional C storage potential of different C-rich substrates (Juncus straw or Juncus-derived biochar) and/or FeSO4 amendments, with a low water table (LW; −15 cm) and high-water table (HW; 0 cm) in intact soil columns (20 cm diam. x 25 cm deep) extracted from degraded upland peat. GHG fluxes, soluble nutrients, changes in microbial community structure and enzyme activity were measured over a one-year period to evaluate the net C storage and their overall GGR potential. HW reduced CO2 emissions by 28 % compared to LW, while CH4 emissions increased, ultimately contributing 61 % of the overall CO2 equivalent (CO2eq) GHG emissions in HW cores with no amendments. Organic amendments had a significant effect on CO2 and CH4 emissions with the highest cumulative emissions being from the Straw-HW (26.2 t CO2eq ha−1 yr−1) and the lowest cumulative emissions being from the Biochar + FeSO4+HW (7.9 t CO2eq ha−1 yr−1). Biochar + FeSO4+HW led to the strongest net gain in soil C, suppressing decomposition of the native peat-C as well as CH4 emissions. The application of FeSO4 significantly reduced CO2eq GHG emissions by preventing methanogenesis through alternative electron acceptors. The Biochar + HW treatment suppressed Ascomycota abundance by 22 %. The combination of a high-water level, biochar addition and availability of alternative electron acceptors (e.g., FeSO4) can increase net C accumulation and GGR via both abiotic and biotic mechanisms, including i) increased C input, ii) modulation of soil microbiome to reduce peat turnover; and iii) suppression of CH4 and N2O emissions.
期刊介绍:
Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.